Thermal stability of fayalite (Fe2SiO4) is studied at hydrogen pressures up to 7.5 GPa and temperatures up to 400 °C. Powder samples of Fe2SiO4 were exposed to a hydrogen or deuterium atmosphere for 24 h in the Toroid-type apparatus at pre-selected pressures and temperatures followed by quenching to the temperature of liquid nitrogen. The phase and chemical compositions of the quenched samples were examined by energy-dispersive X-ray spectroscopy, X-ray diffraction and Raman spectroscopy at ambient pressure. The chemical composition of volatile products was studied by quadrupole mass spectroscopy in the course of heating from − 196 to 20 °C in a pre-evacuated quartz tube. In these experiments, deuterated samples were used to be sure that the detected compounds could only be formed in the reaction of fayalite with the high-pressure D2 gas. The obtained data allowed us to construct the line of thermal stability of fayalite at hydrogen pressures up to 7.5 GPa. The decomposition temperature of fayalite was proved to nonlinearly decrease from ~ 375 °C at the pressures PH2 = 1.4–2.8 GPa to ~ 175 °C at PH2 = 7.5 GPa. At higher temperatures, fayalite fully decomposed to a mixture of silica, water and metallic Fe or FeH depending on the pressure and temperatures of the hydrogenation.